Answer:
An arena stage is a form of the platform in which the area where the actors perform is placed in the center of the audience.
An advantage of this type of stage is that, as it placed in the center all the audience can have a good look at what is happening there.
A disadvantage of the arena stage is that if the play is not prepared properly to be acted in those types of stages some parts of the audience would be seeing the play from the back.
Explanation:
It is also known as theater in the round and it can be traced up to the ancient Greek rituals which then evolved to Greek theater. In this type of stage, the audience surrounds the actors, who perform the play in an acting area at floor level.
I hope this answer helps you.
Answer:
optical
Explanation:
Polarization fall under optical property of material.
Polarization is a property of certain electromagnetic waves in which the direction and the magnitude of electric field are related in some way. Plane polarized light consist of waves in which direction of vibration of waves is same for all waves. Light may be polarized by reflection or by passing it through filters.
Answer:
B. focus, epicenter
Explanation:
the earthquake point where is originates is called the focus of the earthquake and the point in the surface is called the epicenter of the earthquake and this is located exactly above the focus,in this part the earthquake waves reach for the first time
in this case the answer is B
1. In the middle of the continents
The oldest rocks on our planet can be found in the middle of the continental masses. Such places are the interior of Australia, from where the oldest rock have actually been found, Siberia, Central Africa, the interior of Canada, the interior of Brazil... The reason why this is the case is because of the subduction that occurs between the plates. The oceanic plates are the ones that subduct, thus their crust is getting destroyed, so their rocks are younger. The continental plates, on the other hand, are not getting subducted, but instead they either collide with other continental plates, or go above the oceanic plates that subduct below them, thus their crust is usually not destroyed, except on the surface part where the weathering and erosion are taking part.
2. at conservative boundaries
The conservative plate boundaries, more commonly referred to as transform plate boundaries, are the ones where the tectonic plates are sliding past each other. Instead of the plates moving toward each other, or away from each other, at these boundaries the plates are moving in sliding past each other while moving in opposite directions. The pressure between the plates on these boundaries results in cracks in the crust, known as faults, and they are parallel to the plate boundary. Also, these boundaries are very active geologically, and they often cause earthquakes to occur in the surrounding area.